Hostname: page-component-848d4c4894-4rdrl Total loading time: 0 Render date: 2024-06-19T12:02:46.300Z Has data issue: false hasContentIssue false
  • English
  • Français

Flocculation of Selected Clays by Various Electrolytes

Published online by Cambridge University Press:  01 January 2024

Huey-rong Hsi  and
Donald F. Clifton
Huey-rong Hsi*
Affiliation:
College of Mines, University of Idaho, Moscow, Idaho, USA
Donald F. Clifton
Affiliation:
College of Mines, University of Idaho, Moscow, Idaho, USA
*
1Present address: Thompson Products Division of Thompson-Ramo-Wooldridge, Inc., Cleveland, Ohio
Get access Rights & Permissions [Opens in a new window]

Abstract

The flocculation behavior of clay specimens from altered basalt, altered granodiorite, and a transported (?) deposit in Latah County, Idaho, was investigated in order to determine if flocculation behavior would be an aid in characterizing clay samples in a way that could be related to the origin and history of the clays. The clay minerals are of the kaolinite group.

As flocculants, various chlorides differ one hundred-fold and sodium salts twenty-fold in the concentrations necessary to flocculate a clay to a fixed settling rate. The concentrations of individual chlorides necessary to flocculate different clays vary three-fold and the concentrations of individual sodium salts vary ten-fold. In all cases the higher the valence of the cation the lower is the concentration required for flocculation; the relative effectiveness, however, varies with the clay. The relative effectiveness of the anions as flocculants varies greatly with the clay and no definite order of effectiveness is apparent.

Halloysite requires less electrolyte for flocculation and has a larger settling volume than kaolinite. Well crystallized kaolinite has a smaller settling volume than poorly crystallized kaolinite.

Wide differences of flocculation behavior may provide a valuable, rapid method of classifying the clays of a district.

Type
General Session
Information
Clays and Clay Minerals (National Conference on Clays and Clay Minerals) , Volume 9 , February 1960 , pp. 269 - 275
Copyright
Copyright © The Clay Minerals Society 1960

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

Footnotes

Work done under Special Research Project. 60 of the University of Idaho in co operation with the Idaho Bureau of Mines and Geology.

References

Brindley, G. W. (1958) Ion exchange in clay minerals: in Ceramic Fabrication Processes (edited by Kingery, W. D.): John Wiley & Sons, Inc., New York, pp. 7–23.Google Scholar
Grim, R. E. (1953) Clay Mineralogy: McGraw-Hill Book Co. Inc., New York, 384 pp.Google Scholar
Hubbard, C. R. (1957) Mineral resources of Latah County: Idaho Bur. Mines and Geology, County Rept. 2, 29 pp.Google Scholar
Michaels, A. S. (1958) Rheological properties of aqueous clay suspensions: in Ceramic Fabrication Processes (edited by Kingery, W. D.): John Wiley & Sons, Inc., New York, pp. 23–31.Google Scholar
Searle, A. B. and Grimshaw, R. W. (1959) The Chemistry and Physics of Clays: Interscience, New York, 942 pp.Google Scholar